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Programa e Resumos - I Congresso Ibérico de Ciência do Solo 2004

Programa e Resumos - I Congresso Ibérico de Ciência do Solo 2004

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I <strong>Congresso</strong> Ibérico da Ciência <strong>do</strong> <strong>Solo</strong> – 15 a 18 <strong>de</strong> Junho <strong>de</strong> <strong>2004</strong>, Bragança, Portugal<br />

Distribution of Pb ad<strong>de</strong>d to soils from calcareous parent material.<br />

Isaura Rábago 1 , José Ramón Quintana 2 , Ana María Moreno 2 & Juana González 2<br />

1 CIEMAT, Avda. Complutense 22, 28040 Madrid, Spain – Tel: (34) 91 3466206 – E-mail:<br />

isaura.rabago@ciemat.es<br />

2 Dpto. <strong>de</strong> Edafología, Facultad <strong>de</strong> Farmacia, Universidad Complutense, 28040 Madrid, Spain –<br />

Tel: (34) 91 3941759 – E-mail: jrquinta@farm.ucm.es<br />

Resumo<br />

Comunicação: Painel<br />

The main objective of this work was to study the Pb distribution, by applying a<br />

sequential extraction procedure, in or<strong>de</strong>r to i<strong>de</strong>ntify the processes that influence metal<br />

mobility and retention in soils <strong>de</strong>veloped from calcareous materials.<br />

Two groups of samples were collected, from non-polluted forested areas of Quercus<br />

rotundifolia, according to their carbonate content: soils with no carbonates and soils<br />

with carbonates.<br />

Distribution experiments were carried out adding 200 mg L -1 and 50 mg L -1 of Pb (1:10<br />

soil/ solution) to samples in batch experiments. Retention analyses were carried out<br />

applying the Tessier sequential extraction procedure.<br />

All the soil samples had a pH above the neutrality. There were a group of soils with no<br />

carbonates and samples with a content in carbonates between 22 and 63%. The organic<br />

matter contents were similar for both groups of soils. The CEC and the percentages of<br />

clay were higher for the non- carbonated soils.<br />

In both treatments of contamination, the carbonates and the iron and manganese oxi<strong>de</strong>s<br />

are the main fractions involved in the retention of Pb, in<strong>de</strong>pen<strong>de</strong>ntly of the ad<strong>de</strong>d<br />

concentration. The soluble fraction was very low (

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